Tens of gigawatts of heat in Devonian aquifers, priced against a C$44/MWh power pool.
The AGS Geothermal Atlas estimates 4 trillion GJ of heat in place in the Leduc Formation alone (66 GW thermal, 9 GW electrical gross). Gradients average 33 °C/km and reach 36 °C/km in the Hinton–Edson deep basin where Devonian aquifers exceed 120 °C below 3.5 km. The obstacle is cost: AER puts geothermal supply at C$236–278/MWh against a 2025 pool average of C$44.
Gradient above 35 °C/km with 4–6 km of sediment (Hinton–Edson, Peace River Arch)
Permeable reef or Granite Wash aquifers yielding over 80 kg/s at 87–123 °C (3.1–4.1 km)
Basement above 180 °C in western Alberta with high unconfined strength (brittle)
Dense legacy well control that de-risks drilling
Prospectivity envelopes on the map (1)
Deep basin thermal maximum (Hinton–Fox Creek–Grande Prairie)Highly favourable
Hot sedimentary aquifer (Leduc, Swan Hills, Granite Wash) and closed-loop targets · 3K–5K m
Geothermal gradient 35–45 °C/km with Devonian aquifers > 120 °C below 3,500 m
Permeable reef carbonates or basal Granite Wash for conventional doublets
Dense well control lowers drilling risk; Eavor-Loop demonstrates closed loop near Hinton
Source: AGS Geothermal Atlas of Alberta; Alberta No.1 (Greenview) and Eavor projects.
DATASETS THAT TEST THE TARGET
Stack these layers on the integrated map
Discriminating datasets first, then every catalogued public dataset tagged to this commodity. Verified endpoints draw directly; link-only entries open the publisher page.
Subsurface temperature points (BHT-derived)Alberta Geological Survey · Geothermal · drawable · verifiedThermal gradient for geothermal doublets and for DLE kinetics in lithium brines; basement temperature grids exist as LERC tiles.Source ↗
3D Provincial Geological Framework: Precambrian subcrop zonesAlberta Geological Survey · Structure, depth & isopach · drawable · verifiedEntry point to the provincial 3D framework: which Paleozoic zone sits on basement controls helium traps, brine aquifers and storage seals.Source ↗
3D PGF depth-to-Precambrian grid (LERC, link only)Alberta Geological Survey · Structure, depth & isopach · link only · verifiedBasement depth controls geothermal gradient, helium source proximity and basin-centred gas pressure.Source ↗
Active producing wells (Alberta Energy Geoview)Alberta Energy and Minerals · Wells · link only · verifiedWhere hydrocarbons are flowing today: live reservoir pressure, produced-water (brine) access, helium-bearing gas streams and infrastructure for re-entry.Source ↗
Geothermal agreements (live)Alberta Energy and Minerals · Mineral tenure · drawable · verifiedWhere geothermal rights have been staked.Source ↗
Precambrian magnetic basement domains (AGS)Alberta Geological Survey · Aeromagnetics · drawable · verifiedCraton architecture for diamonds (thick cold lithosphere), radiogenic basement for helium, and shear zones for uranium and gold.Source ↗
FutEra Swan Hills geothermal–gas hybridGeothermal · FutEra Power (Razor / AIMCo) · 21 MW hybrid; Canada's only geothermal power plantOperating (2026)Closed-loop pilot funded C$5 M by ERA (Mar 2026).Source ↗
Eavor-Lite closed-loop demo (Rocky Mountain House)Geothermal · Eavor Technologies · Demo 2019–2024; commercial Eavor-Loop in Germany (Dec 2025)Closed (recent) (2026)C$8 M ERA award (Jul 2026) for Eavor-Jules superhot drilling.Source ↗
Latitude 53 geothermal greenhouse (Hinton)Geothermal · Novus Earth · ≈3 MWe + greenhouse heatPermitting (2026)Named by AER as a growth project.Source ↗